Infrared and millimetre-wave scintillometry in the suburban environment – Part 1: Structure parameters

Scintillometry, a form of ground-based remote sensing, provides the capability to estimate surface heat fluxes over scales of a few hundred metres to kilometres. Measurements are spatial averages, making this technique particularly valuable over areas with moderate heterogeneity such as mixed agricu...

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Main Authors: H. C. Ward, J. G. Evans, C. S. B. Grimmond, J. Bradford
Format: Article
Language:English
Published: Copernicus Publications 2015-03-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/8/1385/2015/amt-8-1385-2015.pdf
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author H. C. Ward
J. G. Evans
C. S. B. Grimmond
J. Bradford
author_facet H. C. Ward
J. G. Evans
C. S. B. Grimmond
J. Bradford
author_sort H. C. Ward
collection DOAJ
description Scintillometry, a form of ground-based remote sensing, provides the capability to estimate surface heat fluxes over scales of a few hundred metres to kilometres. Measurements are spatial averages, making this technique particularly valuable over areas with moderate heterogeneity such as mixed agricultural or urban environments. In this study, we present the structure parameters of temperature and humidity, which can be related to the sensible and latent heat fluxes through similarity theory, for a suburban area in the UK. The fluxes are provided in the second paper of this two-part series. A millimetre-wave scintillometer was combined with an infrared scintillometer along a 5.5 km path over northern Swindon. The pairing of these two wavelengths offers sensitivity to both temperature and humidity fluctuations, and the correlation between wavelengths is also used to retrieve the path-averaged temperature–humidity correlation. Comparison is made with structure parameters calculated from an eddy covariance station located close to the centre of the scintillometer path. The performance of the measurement techniques under different conditions is discussed. Similar behaviour is seen between the two data sets at sub-daily timescales. For the two summer-to-winter periods presented here, similar evolution is displayed across the seasons. A higher vegetation fraction within the scintillometer source area is consistent with the lower Bowen ratio observed (midday Bowen ratio < 1) compared with more built-up areas around the eddy covariance station. The energy partitioning is further explored in the companion paper.
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spelling doaj.art-6601d91b0f5e47ffb29ea48472a23cb02022-12-21T21:14:57ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-03-01831385140510.5194/amt-8-1385-2015Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parametersH. C. Ward0J. G. Evans1C. S. B. Grimmond2J. Bradford3Centre for Ecology and Hydrology, Wallingford, Oxfordshire, OX10 8BB, UKCentre for Ecology and Hydrology, Wallingford, Oxfordshire, OX10 8BB, UKDepartment of Geography, King's College London, London, WC2R 2LS, UKSpace Science Department, Rutherford Appleton Laboratory, Didcot, Oxfordshire, OX11 0QX, UKScintillometry, a form of ground-based remote sensing, provides the capability to estimate surface heat fluxes over scales of a few hundred metres to kilometres. Measurements are spatial averages, making this technique particularly valuable over areas with moderate heterogeneity such as mixed agricultural or urban environments. In this study, we present the structure parameters of temperature and humidity, which can be related to the sensible and latent heat fluxes through similarity theory, for a suburban area in the UK. The fluxes are provided in the second paper of this two-part series. A millimetre-wave scintillometer was combined with an infrared scintillometer along a 5.5 km path over northern Swindon. The pairing of these two wavelengths offers sensitivity to both temperature and humidity fluctuations, and the correlation between wavelengths is also used to retrieve the path-averaged temperature–humidity correlation. Comparison is made with structure parameters calculated from an eddy covariance station located close to the centre of the scintillometer path. The performance of the measurement techniques under different conditions is discussed. Similar behaviour is seen between the two data sets at sub-daily timescales. For the two summer-to-winter periods presented here, similar evolution is displayed across the seasons. A higher vegetation fraction within the scintillometer source area is consistent with the lower Bowen ratio observed (midday Bowen ratio < 1) compared with more built-up areas around the eddy covariance station. The energy partitioning is further explored in the companion paper.http://www.atmos-meas-tech.net/8/1385/2015/amt-8-1385-2015.pdf
spellingShingle H. C. Ward
J. G. Evans
C. S. B. Grimmond
J. Bradford
Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
Atmospheric Measurement Techniques
title Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
title_full Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
title_fullStr Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
title_full_unstemmed Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
title_short Infrared and millimetre-wave scintillometry in the suburban environment &ndash; Part 1: Structure parameters
title_sort infrared and millimetre wave scintillometry in the suburban environment ndash part 1 structure parameters
url http://www.atmos-meas-tech.net/8/1385/2015/amt-8-1385-2015.pdf
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